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9 <br />• and interrupted ditches cross the twv forties. Soils are inter- <br />mittently watered and srnietimes temporarily water-logged belay <br />these ponds and along the drain in the west side of SW; SE ;. <br />This does not seem to have miaterially changed the character of the <br />soil. If relocation of water flora is provided and the irrigation <br />dis~ntinued, stripping of this tract should not encounter restrio- <br />five water problems. There is a hydrology plan for relocation of <br />these ditches. <br />Tt~ SOUS <br />A previous soil survey was made try the Soil Conservation Service <br />(SCS) using aerial photos flown 7/22/'75. (Exhibit C-5 Soils <br />Map undated.) This shower: soil 5804, Shawano clay loam, as the <br />daninant soil with soil 1004, Chapin clay loam, occurring in the <br />rnrthwest part of the tract and soil 9904, Persayo-Shavano clay <br />looms occurring on isolated ridges of steeper slopes. This miap <br />• is not shown here. <br />Our Pxamination of the tract indicates that 5810, Shawano fine <br />sandy loam and sandy clay loam, .is the dominant soil on the gentler <br />slopes and that 5804, Shawano sandy clay loam, eroded phase, is <br />more limited to steeper slopes and eroded or disturbed areas. The <br />soil areas shoran as 9904 are Persayo clay loam and sandy clay loam. <br />The soil 1004, Chapin clay loam was not mapped as the conditions <br />found are not typical of the Chapin series. The Chapin series <br />contains much crore clay and is correlated as fine, imntmorilli- <br />nitic, mPSic, aridic Argiustoll. A description of the soils as <br />mapped follows. <br />5810 Shawano sandy clay loam, Slopes 2-5(10.85 acres), C <br />1/ <br />Shawano sandy clay loam is a fine loamy, mixed, frigid,(ustic)Cam- <br />borthid. The topsoil which has been disturbed try cultivation, is <br />a sandy clay loam, dark brawn (7.SYR5/4) dry, and strong brown (7.SYR4/4) <br />1/Near borollic but lighter in color. <br />